New Porphyry Copper–Molybdenum Ore Occurrence in Arganaty Granites of the Eastern Balkhash (Kazakhstan): Geology, Geochemistry, and Mineralogy

Author:

Baibatsha Adilkhan1,Vikentyev Ilya2ORCID,Muratkhanov Daulet1ORCID,Bulegenov Kanat1

Affiliation:

1. Department of Geological Survey, Search and Exploration of Mineral Deposits, Geology and Oil-Gas Business Institute Named after K. Turyssov, Satbayev University, 22 Satbaev Str., Almaty 050013, Kazakhstan

2. Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry, Russian Academy of Sciences (IGEM RAS), Staromonetny Per. 35, 119017 Moscow, Russia

Abstract

In the Balkhash region of Kazakhstan, there are numerous copper and copper–molybdenum deposits, including superlarge Aktogay, Aidarly, Kounrad, and large Sayak deposits. Despite the proximity to these ore districts, the Arganaty district of the Eastern Balkhash region has not attracted significant interest in terms of exploration for many years. Our recent work has identified previously undetected copper–molybdenum mineralization in the granites of the Arganaty massif and has provided a new perspective on the economic potential of this area. In this study, based on the geology, mineralogy, and geochemistry of the Arganaty granites using data from XRF and ICP-MS methods, we reassessed the geological structure and prospectivity of this area. Our investigations have found that the intrusive rocks of the Arganaty massif belong to I-type granites and were formed in a subduction setting rather than a collision setting, as was previously believed. This also indicates the high prospects of the territory in the context of the possible discovery of large Cu or Cu–Mo deposits.

Funder

Science Committee of the Ministry of Science and Higher Education of the Republic of Kazakhstan

Publisher

MDPI AG

Reference60 articles.

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2. Kolesnikov, V.V. (1991). Deposits of Non-Ferrous Metals. Series: Balkhash Segment, Gylym. (In Russian).

3. Geochemistry of late Palaeozoic granitoids of the Balkhash metallogenic belt, Kazakhstan: Implications for crustal growth and tectonic evolution of the Central Asian Orogenic Belt;Liu;Intern. Geol. Rev.,2016

4. Bekzhanov, G.R., Koshkin, V.Y., Nikitchenko, I.I., Skrinnik, L.I., Azizov, T.M., and Timush, A.V. (2000). Geological Structure of Kazakhstan, Academy of Mineral Resources of the Republic of Kazakhstan. (In Russian).

5. Paleozoic crustal growth and metallogeny of Central Asia: Evidence from magmatic-hydrothermal ore systems of Central Kazakhstan;Heinhorst;Tectonophysics,2000

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